J. H. Johnson
1964, Professional Paper 403-G
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateDavis W. Ellis, Howard E. Allen, Allen W. Noehre
1964, Hydrologic Atlas 86
No abstract available....
Davis W. Ellis, Howard E. Allen, Allen W. Noehre
1964, Hydrologic Atlas 85
No abstract available....
M. A. Lopez
1964, Hydrologic Atlas 128
No abstract available....
George A. Dinwiddie, Ward Sundt Motts
1964, Water Supply Paper 1576-E
The need for additional water has increased in recent years on the Acoma and Laguna Indian Reservations in west-central New Mexico because the population and per capita use of water have increased; the tribes also desire water for light industry, for more modern schools, and to increase their irrigation program....
Clarence R. Gilbert, G.G. Commons, G. E. Koberg, F.W. Kennon
1964, Water Supply Paper 1779-F
This report presents the results of an investigation into the effects of floodwaterretarding structures in the 39 square miles of the Honey Creek basin above the stream-gaging station near McKinney, during the period October 1952 to September 1959. The number of such structures in the study area was increased from...
A.I. Johnson
1964, Open-File Report 63-64
E. E. Harris, S. E. Rantz
1964, Water Supply Paper 1591-B
This report presents the results of an investigation of the effect of urban growth on the streamflow regimen of Permanente Creek in Mountain View, Santa Clara County, Calif. The data available did not permit a complete study of all hydrologic aspects, but there is conclusive evidence that the volume of...
George R. Schiner, Robert Schneider
1964, Water Supply Paper 1669-R
The Redwood Falls area includes about 80 square miles in southwestern Minnesota and is about 100 miles west of Minneapolis and St. Paul. Its surface is a gently undulating glacial-drift plain, interrupted in part by the large Minnesota River valley and the tributary Redwood River valley. The drift plain was...
Marvin Arthur Pistrang, Fred Kunkel
1964, Water Supply Paper 1779-Y
No abstract available....
S. E. Rantz
1964, Water Supply Paper 1758
George C. Taylor, P.K. Ghosh
1964, Water Supply Paper 1608-D
The present report is based on a geological and hydrological reconnaissance during 1954 of the Malabar Coastal Plain and adjacent island area of southern Kerala to evaluate the availability of ground water for coastal villages and municipalities and associated industries and the potentialities for future development. The work was done...
George C. Taylor, H.M. Osa, A. Mitra, B.N. Sen
1964, Water Supply Paper 1608-B
This report is based on an investigation of the availability of ground-water supplies in the Bhachau area for the nearby Kandla Port and township development undertaken by the Government of India. This seaport lies on an estuary of the Gulf of Kutch in western India and in the eastern part...
N.C. Matalas, Barbara Jacobs
1964, Professional Paper 434-E
A linear regression for a short and long sequence of hydrologic events is used to lengthen the short sequence. The lengthened sequence consists of the original observations and regressed values plus noise, where the noise is a random variable with zero mean and variance proportional to the variance of the...
John Augustus Baker
1964, Water Supply Paper 1669-Y
Roger Milton Waller
1964, Water Supply Paper 1779-D
R. C. Baker, Leon S. Hughes, I. D. Yost
1964, Water Supply Paper 1669-CC
The average daily load of the Brazos River at Possum Kingdom Reservoir is about 2,800 tons of dissolved solids, of which 1,000 tons is chloride. More than 85 percent of the chloride load is contributed by the Salt Fork Brazos River, and more than 50 percent of the chloride load...
Vernon Kenneth Berwick, Joseph M. Childers, M.A. Kuentzel
1964, Circular 493
This report presents a method for evaluating the magnitude and frequency of floods on the basis of the analysis of flood records. One composite frequency curve is applied to the entire study region. This curve relates floods of various magnitudes at any site within the region to probable recurrence intervals...
M. S. Bedinger, H. G. Jeffery
1964, Water Supply Paper 1669-V
Ivan Barnes, W.T. Stuart, D.W. Fisher
1964, Professional Paper 473-B
Leo T. McCarthy Jr., Walter B. Keighton
1964, Water Supply Paper 1779-X
Water in the Delaware River at Trenton, NJ, is a mixture of several types--water from the mountainous headwater region, water from the coal-mining regions, and water from the limestone valleys. The quantities of these types of water, in relation to the total quantity of water at Trenton, vary with changes...
Edwin P. Weeks
1964, Water Supply Paper 1783
F.A. Welder, R.D. Reeves
1964, Water Supply Paper 1584
The principal aquifer in Uvalde County is the Edwards and associated limestones of Cretaceous age. The aquifer underlies an extensive area in south-central Texas extending along the Balcones fault zone from Kinney County eastward to San Antonio, and thence northeastward to Hays County. The hydrologic unit making up the Edwards...
Frederick K. Mack, F. H. Pauszek, John R. Crippen
1964, Water Supply Paper 1747
This report describes the geology, ground-water conditions, streamflow characteristics, and quality of water in the West Milton area, Saratoga County, N.Y. The West Milton area is in the east-central part of New York in the hilly region that forms a transition zone between the Adirondack Mountains and the Hudson-Mohawk valley...
Natalie D. White
1964, Water Supply Paper 1669-F